The connection between trends of mean temperature and circulation at the surface: Part III. Spring

Jill Williams, Harry van Loon

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The sign of the weighted temperature change over two periods (1950–64, 1942–72) for 15°–80°N was determined by the change in the polar region in spring and autumn, as it was in winter but not in summer. Each of the four seasons shows a different distribution of zonally averaged temperature changes.
Original languageEnglish
Pages (from-to)1591-1596
Number of pages6
JournalMonthly Weather Review
Issue number12
Publication statusPublished - 1976

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